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首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing. >Bayesian-Deep-Learning Estimation of Earthquake Location From Single-Station Observations
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Bayesian-Deep-Learning Estimation of Earthquake Location From Single-Station Observations

机译:单站观测的贝叶斯 - 深探测地震位置

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We present a deep-learning method for a single-station earthquake location, which we approach as a regression problem using two separate Bayesian neural networks. We use a multitask temporal convolutional neural network to learn epicentral distance and P travel time from 1-min seismograms. The network estimates epicentral distance and P travel time with mean errors of 0.23 km and 0.03 s and standard deviations of 5.42 km and 0.66 s, respectively, along with their epistemic and aleatory uncertainties. We design a separate multi-input network using standard convolutional layers to estimate the back-azimuth angle and its epistemic uncertainty. This network estimates the direction from which seismic waves arrive at the station with a mean error of 1°. Using this information, we estimate the epicenter, origin time, and depth along with their confidence intervals. We use a global data set of earthquake signals recorded within 1° (~112 km) from the event to build the model and demonstrate its performance. Our model can predict epicenter, origin time, and depth with mean errors of 7.3 km, 0.4 s, and 6.7 km, respectively, at different locations around the world. Our approach can be used for fast earthquake source characterization with a limited number of observations and also for estimating the location of earthquakes that are sparsely recorded—either because they are small or because stations are widely separated.
机译:我们为单站地震地区提出了一种深入学习的方法,我们使用两个独立的贝叶斯神经网络作为回归问题。我们使用多任务时间卷积神经网络来从1分钟的地震图中学习震中距离和P行程时间。该网络估计Epicentral距离和P旅行时间,平均误差为0.23km,0.03秒,标准偏差分别为5.42km和0.66秒,以及其认识和梯级的不确定性。我们使用标准卷积层设计一个单独的多输入网络,以估计后方角及其认知不确定性。该网络估计地震波到达车站的方向,其平均误差为1°。使用这些信息,我们估计震中,原始时间和深度以及他们的置信区间。我们使用在1°(〜112km)内录制的全局数据集从事件中建立模型并展示其性能。我们的模型可以预测震中,原始时间和深度,平均误差为7.3公里,0.4秒,6.7公里,在世界各地的不同地点。我们的方法可用于快速地震源表征,具有有限数量的观察,并且还用于估算稀疏记录的地震的位置 - 因为它们很小,或者是由于站被广泛分离。

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